Torvosaurus
Torvosaurus | |
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Mounted T. tanneri skeletal reconstruction, Museum of Ancient Life
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Scientific classification | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Chordata |
Clade: | Dinosauria |
Clade: | Saurischia |
Clade: | Theropoda |
Family: | †Megalosauridae |
Subfamily: | † Megalosaurinae
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Genus: | †Torvosaurus Galton & Jensen, 1979 |
Type species | |
†Torvosaurus tanneri Galton & Jensen, 1979
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Other species | |
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Synonyms | |
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Torvosaurus (
In 1979, the
Discovery
Fossilized remains of Torvosaurus have been found in
More remains of a large
In 1971, Vivian Jones of
In 1985, Jensen could report a considerable amount of additional material, among it being the first skull elements.[12] The fossils from Colorado were further described by Brooks Britt in 1991.[13] The holotype, BYU 2002, originally consisted of upper and lower arm bones. The paratypes included some back bones, hip bones, and hand bones.[10] When the material described in 1985 is added, the main missing elements are the shoulder girdle and the thighbone.[13] The original thumb claw, specimen BYUVP 2020, was only provisionally referred, as it had been found in a site 195 kilometers (121 mi) away from the Dry Mesa Quarry.[10] The holotype and paratypes represented at least three individuals, these being two adults and a juvenile.[13] In 1991, Britt concluded that there was no proof that the front limbs of the holotype were associated and chose the left humerus as the lectotype.[13] Several single bones and teeth found in other American sites have been referred to Torvosaurus.[13]
In 1992, fossils of a large theropod found at
In 2012, a still undescribed, 55% complete specimen was discovered in Colorado in the Skull Creek Quarry, which is an exposure of the Morrison Formation. The specimen, nicknamed "Elvis", included the pelvic, spine, and hind limb bones, a complete, associated backbone, as well as cranial elements. It is the most complete specimen of Torvosaurus found to date.[20] A mounted skeleton of the specimen, with missing parts reconstructed with casts from other Torvosaurus specimens, is currently on display in the Museum of Natural History & Science in Cincinnati.[20][21]
In 2000, material from Portugal was referred to a Torvosaurus sp. by Octávio Mateus and Miguel Telles Antunes.[22] In 2006, fossils from the Portuguese Lourinhã Formation were referred to Torvosaurus tanneri.[3] In 2012, however, Matthew Carrano et al. concluded that this material could not be more precisely determined than a Torvosaurus sp.[23] In 2013 and 2014, eggs with and without embryos were reported from Portugal and referred to Torvosaurus.[24][25] The species from Portugal was named T. gurneyi in honor of James Gurney in 2014, the creator of the Dinotopia series of books. It is the largest named theropod known from Europe, although an isolated anterior caudal vertebra from the Vega Formation in Spain, which may belong to Torvosaurus or a closely related taxon, is about 15% larger than the one found on T. gurneyi.[2][26] It was the morphological distinctiveness of the holotype maxilla ML1100 that led to the naming of the Portuguese species.[2] In 2017, a set of Portuguese cranial material assigned to Torvosaurus was described, including a specimen interpreted as belonging to the same individual as the holotype of Torvosaurus gurneyi.[27]
In 2020, Soto et al. described FC-DPV 2971, a tooth from Uruguay, as belonging to a new unnamed species of Torvosaurus.[6] They also assigned Megalosaurus/Ceratosaurus ingens (specimen MB R 1050) from Tanzania to Torvosaurus.[6] Also in 2020, a fragmentary maxilla referable to Torvosaurus was described from the middle Callovian Ornatenton Formation of Germany. This is the oldest record of the genus and suggests that megalosaurines originated in Europe, or at least that Europe was a biogeographical turntable for them from the Middle to the early Late Jurassic. Other possible Torvosaurus instances in Europe include fragmentary remains from the Kimmeridge Clay of England that possibly belong to the genus.[1] These consist of a tibia (OUMNH J.29886) and a maxilla fragment that were collected separately from each other.[23]
Description
Torvosaurus was a very large and robust predatory dinosaur, with an estimated maximum body length of 10–11 meters (33–36 ft) and mass of 4–5 metric tons (4.4–5.5 short tons) for the Portuguese species T. gurneyi,[2][3] making T. gurneyi among the largest terrestrial carnivores of the Jurassic. Claims have been made indicating even larger sizes for the American species T. tanneri up to 12 m (39 ft) in length and more than 4 t (4.4 short tons) based on incomplete remains of Edmarka rex and Brontoraptor.[28][16][29] However, these claims regarding T. tanneri are likely erroneous, as the discovered remains of T. tanneri indicate that they reached adult size at 9 meters (30 ft) in length and approximately 2 metric tons (2.2 short tons) in body mass.[13][30][31][32] Furthermore, Edmarka rex and Brontoraptor lack detailed analyses to verify whether or not they actually belong to T. tanneri.[19][16]
Among the differentiating features originally recognized between T. gurneyi and T. tanneri are the number of teeth, alongside the size and shape of the mouth. While the upper jaw of T. tanneri has more than 11 teeth, that of T. gurneyi has less.[2] However, later examination of a new right maxilla, probably belonging to the same individual as the holotype of T. gurneyi, has determined that, while the two species can be distinguished based on the morphology of the maxillary medial wall and interdental plates, the supposedly lower number of maxillary teeth in the Portuguese form may be an artifact of preservation, since it is not possible to know the exact number of teeth in the complete maxilla at the moment.[27]
The material from Germany is further distinguished by the other two species by a temporal difference of c. 10 Ma and a few morphological differences which indicate that it was the third species outside a sister taxon relationship between T. tanneri and T. gurneyi. The material is only 10% smaller than the maxilla of T. tanneri, although the ontogenetic stage of the specimen is unknown. This indicates that derived megalosaurines were already among the largest terrestrial predators of the late Middle Jurassic, with only a moderate increase in size in the genus by the Late Jurassic.[1]
Torvosaurus had an elongated, narrow snout, with a kink in its profile just above the large nostrils. The frontmost snout bone, the
Systematics and classification
When first described in 1979 by Galton and Jensen,
The following is a cladogram based on the phylogenetic analysis conducted by Carrano, Benson, and Sampson (2012) showing the relationships of Torvosaurus:[15]
Megalosauroidea |
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Distinguishing anatomical features
According to Carrano et al. (2012), Torvosaurus can be distinguished based on the following characteristics:[38]
- The presence of a very shallow maxillary fossa (it lacks a fenestra maxillaris piercing the bone wall)
- The presence of fused interdental plates
- The pneumatic fossae in the posterior dorsal and the anterior caudal vertebrae centra being expanded to form enlarged, deep openings
- The puboischiadic plate being highly ossified (the paired bony plates of both sides connect and close off the entire underside of the pelvis, a very basal trait that Galton & Jensen saw as an indication that Theropoda was polyphyletic, with Carnosauria having independently evolved from carnivorous Prosauropoda)[10]
- A distal expansion of the ischium shaft with a prominent lateral midline crest and an ovalur outline when examined in lateral view
- The cervical vertebrae are opisthocoelous with a pronounced flat rim around the anterior ball (according to Rauhut, 2000)
- A transverse fenestra is situated in the neural arch of the dorsal vertebrae in front of the hyposphene (according to Rauhut, 2000)[39]
Paleobiology
The study of fossilized embryos of Torvosaurus provides researchers with information about the transformation of the embryo over time, the different developmental pathways present in dinosaur lineages, dinosaur reproductive behavior, and dinosaur parental care.[40][41][42] In 2013, Araújo et al. announced the discovery of specimen ML1188, a clutch of crushed dinosaur eggs and embryonic material attributed to Torvosaurus.[43] This discovery further supports the hypothesis that large theropods were oviparous, meaning that they laid eggs and hence that embryonic development occurred outside the body of female dinosaurs. This discovery was made in 2005 by the Dutch amateur fossil-hunter Aart Walen at the Lourinhã Formation in Western Portugal in fluvial overbank sediments that are considered to be from the Tithonian age of the Jurassic, approximately 152 to 145 million years ago. This discovery is paleontologically significant for a number of reasons: (a) these are the most primitive dinosaur embryos known; (b) these are the only basal theropod embryos known; (c) fossilized eggs and embryos are rarely found together; (d) it represents the first evidence of a one-layered eggshell for theropod dinosaurs; and (e) it allows researchers to link a new eggshell morphology to the osteology of a particular group of theropod dinosaurs.[24] The specimen is housed at the Museu da Lourinhã in Portugal. As the eggs were abandoned due to unknown circumstances, it is not known if Torvosaurus provided parental care to its eggs and young or abandoned them shortly after laying.[44] However, the eggshells are highly porous, allowing efficient gaseous exchange between the external and internal media, thus indicating the eggs were buried for incubation within substrate in a manner similar to modern seaturtles. This is also corroborated by the undisturbed taphonomic setting and low-energy geological context.[24]
All documented Torvosaurus specimens from the Morrison Formation are from similarly sized, likely adult individuals and the lack of immature individuals may be explained by many factors, none of which are mutually exclusive. For one thing, the formation is known to preserve large vertebrates better than smaller ones. Immature individuals may also have occupied a different ecological niche from adults in habitats where their remains were likely to preserve as fossils and they may have been the prey of choice of larger predators as well. Torvosaurus may also have experienced Type B1 population survivorship, as has been found in other dinosaurs, with mortality increasing after sexual maturity was achieved, leading to an abundance of mature individuals in the fossil record. A final possibility is that immature Torvosaurus remains could be misidentified due to having different proportions compared to the very large and robust adults.[4]
Paleoecology
Provenance and occurrence
The type specimen of Torvosaurus tanneri, BYU 2002, was recovered in the Dry Mesa Quarry of the Brushy Basin Member of the Morrison Formation in Montrose County, Colorado. The specimen was collected by James A. Jensen and Kenneth Stadtman in 1972 in medium-grained, coarse sandstone that was deposited during the Tithonian and Kimmeridgian ages of the Jurassic, approximately 153 to 148 million years ago.[45] This specimen is housed in the collection of Brigham Young University in Provo, Utah.
Fauna and habitat in North America
Studies suggest that the
The flora of the period has been revealed by fossils of
Fauna and habitat in Europe
The Ornatenton Formation is a Callovian aged shallow marine deposit, within the formation Torvosaurus was sympatric with the closely related and also large Wiehenvenator. The Lourinhã Formation is Kimmeridgian-Tithonian in age. The environment is coastal and therefore has a strong marine influence. Its flora and fauna are very similar to that of the Morrison. Torvosaurus appears to be the top predator here. It lived alongside the European species of Allosaurus (A. europaeus), Ceratosaurus, Stegosaurus, and presumably Camptosaurus. The theropod Lourinhanosaurus also stalked the area. Lusotitan was the largest sauropod in the region, while the diplodocids Dinheirosaurus and Lourinhasaurus were also present. Dacentrurus and Miragaia were both stegosaurs, while Dracopelta was an ankylosaurian. Draconyx was an iguanodontid related to Camptosaurus. Due to the marine nature of the Lourinhã Formation, sharks, plesiochelyid turtles, and teleosaurid crocodyliforms are also present.[48]
Fauna and habitat in Africa
The small-scale trough and ripple cross-bedded fine-grained sandstone at the base of the Upper Dinosaur Member of the Tendaguru Formation, of which possible Torvosaurus material is known from, is interpreted as tidal flat deposits. Stagnant water bodies, such as small lakes and ponds, were present and a freshwater depositional environment close to the sea was also probably present.
The possible unnamed Torvosaurus species from the Tendaguru Formation would have shared its habitat with many species of
Fauna and habitat in South America
Within South America, possible Torvosaurus remains are only present within the
If present, Torvosaurus would probably have been the
Coexistence with other large carnivores
Torvosaurus coexisted with other large theropods such as Allosaurus, Ceratosaurus, and Saurophaganax in the United States, Allosaurus, Ceratosaurus, and Lourinhanosaurus in Portugal, possibly Veterupristisaurus in Tanzania, and possibly cf. Ceratosaurus (?) in Uruguay. The three, possibly four, species appear to have had different ecological niches, based on anatomy and the location of fossils. Torvosaurus and Ceratosaurus may have preferred to be active around waterways and had lower, more sinuous, bodies that would have given them an advantage in forest and underbrush terrains, whereas Allosaurus had shorter bodies, longer legs, were faster and less maneuverable, and seem to have preferred dry floodplains.[53] Also, Rauhut et al. (2016) proposed that allosaurids and megalosaurids would have had different environmental preferences, the former being more common in inland areas, while the latter being dominant in marine and coastal environments.[54]
On the other hand, the majority of Torvosaurus remains from the Morrison Formation have been found in localities preserving multiple taxa, including Allosaurus, with Torvosaurus itself being a minor component of the bonebeds. This pattern has been interpreted as indicative of Torvosaurus sharing habitats with other predators, most notably Allosaurus, but at much lower abundances.[4] The three may also have had different dietary preferences, with Allosaurus being more suited for bone slicing (thanks to its short and stout serrated teeth, deep and narrow skull, and powerful dorsoventral movement capacity of the neck), while Ceratosaurus, with its long and blade-like teeth and relatively straight neck, would have probably been incapable of doing so, instead concentrating on the deepest organs of a carcass. While probably capable of some bone consumption, Torvosaurus, with its large skull and teeth and large, powerful, and lithe body may have been specialized in opening up and dismembering exceptionally large sauropod carcasses. This would have allowed smaller theropods, like Allosaurus, better access in a possible commensalism relationship.[55]
Allosaurus was itself a potential food item to other carnivores, as illustrated by an Allosaurus pubic foot marked by the teeth of another theropod, probably Ceratosaurus or Torvosaurus. The location of the bone in the body (along the bottom margin of the torso and partially shielded by the legs) and the fact that it was among the most massive in the skeleton indicates that the Allosaurus was being scavenged.[56]
Bite marks on Allosaurus and Mymoorapelta remains were found among other bones with feeding traces in the Upper Jurassic Mygatt-Moore Quarry. Unlike the others, these have left striations that, when measured to determine denticle width, produced tooth and body size extrapolations greater than any known specimen of Allosaurus or Ceratosaurus, the two large predators known for osteological remains from the quarry. The extrapolations are instead coherent, either with an unusually large specimen of Allosaurus or a separate large taxon, like Torvosaurus or Saurophaganax, both of which are not known from the quarry. The result either increases the known diversity of the site based on ichnological evidence alone or represents powerful evidence of cannibalism in Allosaurus. Based on the position and nutrient value associated with the various skeletal elements with bite marks, it is predicted that while Mymoorapelta was either predated upon or scavenged shortly after death, Allosaurus was scavenged some time after death.[57]
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